Ontario Geological Survey
Permanent Link to this Record:
MDI52N04SW00103
| Record Name(s) | Peterson - Anomaly D - 1991 |
|---|---|
| Related Record Type | Simple |
| Related Record(s) | |
| Record Status | Discretionary Occurrence |
| Date Created | 1991-Mar-11 |
| Date Last Modified | 2022-Jun-28 |
| Created By | |
| Revised By |
Primary Commodities: Gold
Township or Area: Fairlie
Latitude: 51° 1' 51.59" Longitude: -93° 59' 39.02"
UTM Zone: 15 Easting: 430286.666 Northing: 5653742.055 UTM Datum: NAD83
Resident Geologist District: Red Lake
NTS Grid: 52N04SW
Point Location Description: N/A
Location Method: Conversion from MDI
1972: The Property was held by C.W. Peterson of Red Lake. 1972 - overburden stripping and 2 trenhes were completed - Ronka EM-16 survey completed - Two diamond drill holes completed.
Province: Superior
Subprovince: Uchi
Terrane: North Caribou
Domain: Uchi
Belt: Red Lake
Geological Age: Archean
Metamorphism Type: Regional
Metamorphism Grade: Greenschist
Dec 07, 2005 (K R Kettles) - GEOLOGICAL DESCRIPTION: The oourrence is located west of the Dome Stock and is underlain primarily by altered mafic volcanic rocks. These are composed of tuffs and flows. Pillow structures have been found that indicated the flow tops are to the northwest. Volcanic breccias have also been recognized in the area. Intruding into the volcanics are gabbroic to dioritic dikes. Foliation planes in the volcanic rocks strike approximately NW-SE and dip vertically. Several wide sulphide rich zones have been observed, which contain pyrite, pyrrhotite and chalcopyrite. DEPOSIT DESCRIPTION: A wide shear zone is located on the western end of the island, and it is believed to be the locus for the gold and silver mineralization. Several 3 to 5 cm quartz veins and numerous quartz-carbonate stringers have been noted from drill core. GEOPHYSICAL DATA: A strong EM conductor with good width was discovered and this probably represents a zone of sulphide mineralization.
| Rock Type | Rank | Composition | Texture | Relationship | Vein | 1 | Quartz Vein | Host |
|---|---|---|---|---|
| Mafic Tuff | 2 | Mafic Tuff | Tuff | Adjacent |
| Mafic lava flow-unsubdivided | 3 | Flows | Massive To Pillowed | Adjacent |
| Mafic flow breccia | 4 | Volcanic Breccias | Brecciated | Adjacent |
| Gabbro | 5 | Gabbroic | Dikes | Near |
| Diorite | 6 | Diorite | Dikes | Near |
| Mylonite/Fault Gouge/Pseudotachylite | 7 | Shear Zone | Host |
Dec 07, 2005 (K R Kettles) - The oourrence is located west of the Dome Stock and is underlain primarily by altered mafic volcanic rocks. These are composed of tuffs and flows. Pillow structures have been found that indicated the flow tops are to the northwest. Volcanic breccias have also been recognized in the area. Intruding into the volcanics are gabbroic to dioritic dikes. Foliation planes in the volcanic rocks strike approximately NW-SE and dip vertically. Several wide sulphide rich zones have been observed, which contain pyrite, pyrrhotite and chalcopyrite. A wide shear zone is located on the western end of the island, and it is believed to be the locus for the gold and silver mineralization. Several 3 to 5 cm quartz veins and numerous quartz-carbonate stringers have been noted from drill core.
| Rank | Mineral Name | Class | Economic Mineral Type | Alteration Mineral Type | Alteration Ranking | Alteration Intensity | Alteration Style |
|---|---|---|---|---|---|---|---|
| 1 | Gold | Economic | Ore | ||||
| 2 | Silver | Economic | Ore | ||||
| 3 | Chalcopyrite | Economic | Ore | ||||
| 4 | Pyrite | Economic | Ore | ||||
| 5 | Pyrrhotite | Economic | Ore | ||||
| 1 | Quartz | Economic | Gangue | ||||
| Carbonate | Alteration | Carbonatization | 1 | Weak | Veins | ||
| Quartz | Alteration | Silicification | 2 | Medium | Veins | ||
| Epidote | Alteration | Epidotization | 3 | Medium | Disseminated |
Dec 07, 2005 (K R Kettles) - The oourrence is located west of the Dome Stock and is underlain primarily by altered mafic volcanic rocks. . Several wide sulphide rich zones have been observed, which contain pyrite, pyrrhotite and chalcopyrite: A wide shear zone is located on the western end of the island, and it is believed to be the locus for the gold and silver mineralization. Several 3 to 5 cm quartz veins and numerous quartz-carbonate stringers have been noted from drill core. MDI1 Data: GRADE - GRAB SAMPLE: 0.05 OPT AU. ALSO GOLD VALUES FROM DDH.(FROM OFR 5558).
Dec 07, 2005 (K R Kettles) - The mafic volcanics have been carbonatized, silicified and epidotized.
File - Resident Geologist files AF RL 1972 Fairlie #27
Publication Number: AF RL 1972 Date: 1972
Author: Peterson, C.W.
Publisher Name:
Location: Red Lake RGP
File - Resident Geologist Files AF RL 1986 Fairlie #67, 78
Publication Number: AF RL 1986 Date: 1986
Author:
Publisher Name:
Location: Red Lake RGP
File - Resident Geologist files AF RL 1989 Fairlie #82
Publication Number: AF RL 1989 Date: 1989
Author:
Publisher Name:
Location: Red Lake RGP
Mono - Gold occurrences, prospects, and deposits of the Red Lake area, volumes 1 and 2
Publication Number: OFR5558 Page: 475-476 Date: 1987
Author: Durocher M.E., Burchell P.S., Andrews A.J.
Publisher Name: Ontario Geological Survey
Location:
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